Journal of Geophysical Research Atmospheres · 1980 · 242 citations · 28 references
Natural SciencesEarth SciencesGeophysicsAtmospheric ChemistryAtmospheric ScienceSpectroscopyAtmospheric Trace GasesPlanetary AtmospheresPlanetary CompositionAtmospheric CharacterizationMass Spectrometric DetectionNeutral Gas DynamicsQuadrupole Mass AnalyzersQuadrupole Mass SpectrometrySpectroscopy Of Planetary AtmospheresVenus Atmosphere Chemistry
The neutral gas composition and density in the thermosphere of Venus is being measured with a quadrupole mass spectrometer on the Pioneer Venus orbiter. Data are obtained near periapsis once per day approximately 150–250 km above the surface. The principal gases in the thermosphere are CO 2 , CO, N 2 , O, N, and He. Atomic oxygen is the major constituent above 155 km on the dayside and also on the nightside up to 180 km when helium becomes the major constituent. The average values of CO 2 , CO, N 2 , O, and N remain nearly constant during day and night, but an abrupt change occurs across the terminator from a high dayside value to a low nightside value. The helium density varies in the opposite way, and a distinct bulge was observed at night near the morning terminator. The data have been used as the basis of an empirical model. Large orbit to orbit variations in densities were also observed on the nightside, suggesting perhaps strong turbulent motion in the atmosphere below. Kinetic temperatures inferred from scale heights are approximately 285°K on the dayside and 110°K at night. The average global temperature obtained from the model is 199°K.
28
Some properties of upper atmosphere dynamics
H. G. Mayr, I. Harris, N. W. Spencer · Reviews of Geophysics · 1978 · 271 citations
The upper atmosphere of Venus during morning conditions
U. von Zahn, K. H. Fricke, D. M. Hunten et al. · Journal of Geophysical Research Atmospheres · 1980 · 182 citations
L. Colin · Journal of Geophysical Research Atmospheres · 1980 · 161 citations